<h2><SPAN name="VII"></SPAN>VII</h2>
<p class="h3">READING THE RIDDLES OF THE ROCKS</p>
<div class="inset20">
<p>"<i>And the first Morning of Creation wrote<br/>
What the Last Dawn of Reckoning shall read.</i>"<br/></p>
</div>
<p>It is quite possible that the reader may wish
to know something of the manner in which
the specimens described in these pages have
been gathered, how we acquire our knowledge
of Brontosaurus, Claosaurus, or any of the
many other "sauruses," and how their restorations
have been made.</p>
<p>There was a time, not so very long ago,
when fossils were looked upon as mere sports
of Nature, and little attention paid to them;
later their true nature was recognized, though
they were merely gathered haphazard as occasion
might offer. But now, and for many
years past, the fossil-bearing rocks of many
parts of the world have been systematically
worked, and from the material thus obtained<span class="pagenum"><SPAN name="Page_112">[112]</SPAN></span>
we have acquired a great deal of information
regarding the inhabitants of the ancient world.
This is particularly true of our own western
country, where a vast amount of collecting has
been done, although very much remains to be
done in the matter of perfecting this knowledge,
and hosts of new animals remain to be
discovered. For this information we are almost
as much indebted to the collector who has
gathered the needed material, and the preparator
whose patience and skill have made it
available for study, as to the palæontologist
who has interpreted the meaning of the
bones.</p>
<p>To collect successfully demands not only
a knowledge of the rocks in which fossils
occur and of the localities where they are best
exposed to view, but an eye quick to detect a
piece of bone protruding from a rock or lying
amongst the shale, and, above all, the ability
to work a deposit to advantage after it has
been found. The collector of living animals
hies to regions where there is plenty for bird
and beast to eat and drink, but the collector of
extinct animals cares little for what is on the<span class="pagenum"><SPAN name="Page_113">[113]</SPAN></span>
surface of the earth; his great desire is to see
as much as possible of what may lie beneath.
So the prospector in search of fossils betakes
himself to some region where the ceaseless
warfare waged by water against the dry land
has seamed the face of the earth with countless
gullies and canyons, or carved it into slopes
and bluffs in which the edges of the bone-bearing
strata are exposed to view, and along
these he skirts, ever on the look-out for some
projecting bit of bone. The country is an
almost shadeless desert, burning hot by day,
uncomfortably cool at night. Water is scarce,
and when it can be found, often has little to
commend it save wetness; but the collector is
buoyed up through all this with the hope that
he may discover some creature new to science
that shall not only be bigger and uglier and
stranger than any heretofore found, but shall
be the long-sought form needed for the solution
of some difficult problem in the history
of the past.</p>
<p>Now collecting is a lottery, differing from
most lotteries, however, in that while some of
the returns may be pretty small, there are few<span class="pagenum"><SPAN name="Page_114">[114]</SPAN></span>
absolute blanks and some remarkably large
prizes, and every collector hopes that it may
fall to his lot to win one of these, and is willing
to work long and arduously for the chance of
obtaining it.</p>
<p>It may give some idea of the chances to say
that some years ago Dr. Wortman spent almost
an entire season in the field without success,
and then, at the eleventh hour, found the
now famous skeleton of Phenacodus, or that a
party from Princeton actually camped within
100 yards of a rich deposit of rare fossils and
yet failed to discover it.</p>
<p>Let us, however, suppose that the reconnaissance
has been successful, and that an outcrop
of bone has been found, serving like a tombstone
carven with strange characters to indicate
the burial-place of some primeval monster.
Possibly Nature long ago rifled the grave, washing
away much of the skeleton, and leaving
little save the fragments visible on the surface;
on the other hand, these pieces may form part
of a complete skeleton, and there is no way to
decide this important question save by actual
excavation. The manner of disinterment varies,<span class="pagenum"><SPAN name="Page_115">[115]</SPAN></span>
but much depends on whether the fossil
lies in comparatively loose shale or is imbedded
in the solid rock, whether the strata are level
or dip downward into the hillside. If, unfortunately,
this last is the case, it necessitates a
careful shoring up of the excavation with props
of cotton-wood or such boards as may have
been brought along to box specimens, or it may
even be necessary to run a short tunnel in order
to get at some coveted bone. Should the
specimen lie in shale, as is the case with most
of the large reptiles that have been collected,
much of that work may be done with pick and
shovel; but if it is desirable or necessary to
work in firm rock, drills and hammers, wedges,
even powder, may be needed to rend from Nature
her long-kept secrets. In any event, a
detailed plan is made of the excavation, and
each piece of bone or section of rock duly recorded
therein by letter and number, so that
later on the relation of the parts to one another
may be known, or the various sections assembled
in the work-room exactly as they lay
in the quarry. Bones which lie in loose rock
are often, one might say usually, more or less<span class="pagenum"><SPAN name="Page_116">[116]</SPAN></span>
broken, and when a bone three, four, or even
six feet long, weighing anywhere from 100 to
1,000 pounds, has been shattered to fragments
the problem of removing it is no easy one.
But here the skill of the collector comes into
play to treat the fossil as a surgeon treats a
fractured limb, to cover it with plaster bandages,
and brace it with splints of wood or iron
so that the specimen may not only be taken
from the ground but endure in safety the coming
journey of a thousand or more miles. For
simpler cases or lighter objects strips of sacking,
or even paper, applied with flour and water,
suffice, or pieces of sacking soaked in thin plaster
may be laid over the bone, first covering it
with thin paper in order that the plaster jacket
may simply stiffen and not adhere to it. Collecting
has not always been carried on in this
systematic manner, for the development of the
present methods has been the result of years of
experience; formerly there was a mere skimming-over
of the surface in what Professor
Marsh used to term the potato-gathering style,
but now the effort is made to remove specimens
intact, often imbedded in large masses<span class="pagenum"><SPAN name="Page_117">[117]</SPAN></span>
of rock, in order that all parts may be preserved.</p>
<p>We will take it for granted that our specimens
have safely passed through all perils by
land and water, road and rail; that they have
been quarried, boxed, carted over a roadless
country to the nearest railway, and have withstood
2,000 miles of jolting in a freight-car.
The first step in reconstruction has been taken;
the problem, now that the boxes are reposing
on the work-room floor, is to make the blocks
of stone give up the secrets they have guarded
for ages, to free the bones from their enveloping
matrix in order that they may tell us
something of the life of the past. The method
of doing this varies with the conditions under
which the material has been gathered, and if
from hard clay, chalk, or shale, the process,
though tedious enough at best, is by no means
so difficult as if the specimens are imbedded
in solid rock. In this case the fragments
from a given section of quarry must be assembled
according to the plan which has been
carefully made as the work of exhumation
progressed, all pieces containing bone must be<span class="pagenum"><SPAN name="Page_118">[118]</SPAN></span>
stuck together, and weak parts strengthened
with gum or glue. Now the mass is attacked
with hammer and chisel, and the surrounding
matrix slowly and carefully cut away until the
contained bone is revealed, a process much
simpler and more expeditious in the telling
than in the actuality; for the preparator may
not use the heavy tools of the ordinary stone-cutter:
sometimes an awl, or even a glover's
needle, must suffice him, and the chips cut off
are so small and such care must be taken not
to injure the bone that the work is really tedious.
This may, perhaps, be better appreciated
by saying that to clean a single vertebra
of such a huge Dinosaur as Diplodocus may
require a month of continuous labor, and that
a score of these big and complicated bones,
besides others of simpler structure, are included
in the backbone. The finished specimen
weighs over 120 pounds, while as originally
collected, with all the adherent rock, the
weight was twice or thrice as great. Such a
mass as this is comparatively small, and sometimes
huge blocks are taken containing entire
skulls or a number of bones, and not infrequently<span class="pagenum"><SPAN name="Page_119">[119]</SPAN></span>
weighing a ton. The largest single
specimen is a skull of Triceratops, collected
by Mr. J. B. Hatcher, which weighed, when
boxed, 3,650 pounds.</p>
<p>Or, as the result of some mishap, or through
the work of an inexperienced collector, a valuable
specimen may arrive in the shape of a
box full of irregular fragments of stone compared
with which a dissected map or an old-fashioned
Chinese puzzle is simplicity itself,
and one may spend hours looking for some
piece whose proper location gives the clew to
an entire section, and days, even, may be consumed
before the task is completed. While
this not only tries the patience, but the eyes
as well, there is, nevertheless, a fascination
about this work of fashioning a bone out of
scores, possibly hundreds, of fragments, and
watching the irregular bits of stone shaping
themselves into a mosaic that forms a portion
of some creature, possibly quite new to science,
and destined to bear a name as long as
itself. And thus, after many days of toil, the
bone that millions of years before sank into
the mud of some old lake-bottom or was<span class="pagenum"><SPAN name="Page_120">[120]</SPAN></span>
buried in the sandy shoals of an ancient river,
is brought to light once more to help tell the
tale of the creatures of the past.</p>
<p>One bone might convey a great deal of information;
on the other hand it might reveal
very little; for, while it is very painful to say
so, the popular impression that it is possible to
reconstruct an animal from a single bone, or
tell its size and habits from a tooth is but
partially correct, and sometimes "the eminent
scientist" has come to grief even with a great
many bones at his disposal. Did not one of
the ablest anatomists describe and figure the
hip-bones of a Dinosaur as its shoulder-blade,
and another, equally able, reconstruct a reptile
"hind side before," placing the head on the
tail! This certainly sounds absurd enough;
but just as absurd mistakes are made by men
in other walks of life, often with far more deplorable
results.</p>
<p>Before passing to the restoration of the exterior
of animals it may be well to say something
of the manner in which the skeleton of
an extinct animal may be reconstructed and
the meaning of its various parts interpreted.<span class="pagenum"><SPAN name="Page_121">[121]</SPAN></span>
For the adjustment of the muscles is dependent
on the structure of the skeleton, and putting
on the muscles means blocking out the
form, details of external appearance being supplied
by the skin and its accessories of hair,
scales, or horns. Let us suppose in the present
instance that we are dealing with one of the
great reptiles known as Triceratops whose remains
are among the treasures of the National
Museum at Washington, for the reconstruction
of the big beast well illustrates the methods
of the palæontologist and also the troubles
by which he is beset. Moreover, this is not a
purely imaginary case, but one that is very
real, for the skeleton of this animal which was
shown at Buffalo was restored in papier-maché
in exactly the manner indicated. We have a
goodly number of bones, but by no means an
entire skeleton, and yet we wish to complete
the skeleton and incidentally to form some
idea of the creature's habits. Now we can interpret
the past only by a knowledge of the
present, and it is by carefully studying the
skeletons of the animals of to-day that we can
learn to read the meaning of the symbols of<span class="pagenum"><SPAN name="Page_122">[122]</SPAN></span>
bones left by the animals of a million yesterdays.
Thus we find that certain characters
distinguish the bone of a mammal from that
of a bird, a reptile, or a fish, and these in turn
from one another, and this constitutes the
A B C of comparative anatomy. And, in a
like manner, the bones of the various divisions
of these main groups have to a greater or less
extent their own distinguishing characteristics,
so that by first comparing the bones of extinct
animals with those of creatures that are now
living we are enabled to recognize their nearest
existing relative, and then by comparing them
with one another we learn the relations they
bore in the ancient world. But it must be
borne in mind that some of the early beasts
were so very different from those of to-day
that until pretty much their entire structure
was known there was nothing with which to
compare odd bones. Had but a single incomplete
specimen of Triceratops come to light
we should be very much in the dark concerning
him; and although remains of some thirty
individuals have been discovered, these have
been so imperfect that we are very far from<span class="pagenum"><SPAN name="Page_123">[123]</SPAN></span>
having all the information we need. A great
part of the head, with its formidable looking
horns, is present, and although the nose is
gone, we know from other specimens that it,
too, was armed with a knob, or horn, and that
the skull ended in a beak, something like that
of a snapping turtle, though formed by a separate
and extra bone; similarly the end of the
lower jaw is lacking, but we may be pretty
certain that it ended in a beak, to match that
of the skull. The large leg-bones of our specimen
are mostly represented, for these being
among the more solid parts of the skeleton
are more frequently preserved than any others,
and though some are from one side and some
from another, this matters not. If the hind
legs were disproportionately long it would indicate
that our animal often or habitually
walked erect, but as there is only difference
enough between the fore and hind limbs to
enable Triceratops to browse comfortably from
the ground we would naturally place him on
all fours, even were the skull not so large as to
make the creature too top-heavy for any other
mode of locomotion. Were the limbs very<span class="pagenum"><SPAN name="Page_124">[124]</SPAN></span>
small in comparison with the other bones, it
would obviously mean that their owner passed
his life in the water. For a skeleton has a twofold
meaning, it is the best, the most enduring,
testimony we have as to an animal's place in
nature and the relationships it sustains to the
creatures that lived with it, before it, and after
it. More than this, a skeleton is the solution
of a problem in mechanics, the problem of
carrying a given weight and of adaptation to
a given mode of life. Thus the skeleton varies
according as a creature dwells on land, in the
water, or in the air, and according as it feeds
on grass or preys upon its fellows.</p>
<p>And so the mechanics of a skeleton afford
us a clew to the habits of the living animal.
Something, too, may be gathered from the
structure of the leg-bones, for solid bones mean
either a sluggish animal or a creature of more
or less aquatic habits, while hollow bones emphatically
declare a land animal, and an active
one at that; and this, in the case of the Dinosaurs,
hints at predatory habits, the ability to
catch and eat their defenceless and more sluggish
brethren. A claw, or, better yet, a tooth,<span class="pagenum"><SPAN name="Page_125">[125]</SPAN></span>
may confirm or refute this hint; for a blunt claw
could not be used in tearing prey limb from
limb, nor would a double-edged tooth, made
for rending flesh, serve for champing grass.</p>
<p>But few bones of the feet, and especially the
fore feet, are present, these smaller parts of the
skeleton having been washed away before the
ponderous frame was buried in the sand, and
the best that can be done is to follow the law
of probabilities and put three toes on the hind
foot and five on the fore, two of these last
without claws. The single blunt round claw
among our bones shows, as do the teeth, that
Triceratops was herbivorous; it also pointed a
little downward, and this tells that in the living
animal the sole of the foot was a thick, soft
pad, somewhat as it is in the elephant and rhinoceros,
and that the toes were not entirely
free from one another. There are less than a
dozen vertebræ and still fewer ribs, besides
half a barrelful of pieces, from which to reconstruct
a backbone twenty feet long. That the
ribs are part from one side and part from another
matters no more than it did in the case
of the leg-bones; but the backbone presents a<span class="pagenum"><SPAN name="Page_126">[126]</SPAN></span>
more difficult problem, since the pieces are not
like so many checkers—all made after one pattern—but
each has an individuality of its own.
The total number of vertebræ must be guessed
at (perhaps it would sound better to say estimated,
but it really means the same), and
knowing that some sections are from the front
part of the vertebral column and some from
the back, we must fill in the gaps as best we
may. The ribs offer a little aid in this task,
giving certain details of the vertebræ, while
those in turn tell something about the adjoining
parts of the ribs. We finish our Triceratops
with a tail of moderate length, as indicated
by the rapid taper of the few vertebræ
available, and from these we gather, too, that
in life the tail was round, and not flattened,
and that it neither served for swimming nor
for a balancing pole. And so, little by little,
have been pieced together the fragments from
which we have derived our knowledge of the
past, and thus has the palæontologist read the
riddles of the rocks.</p>
<div class="figcenter"> <ANTIMG src="images/i_172.jpg" width-obs="400" height-obs="273" alt="" /> Fig. 26.—Triceratops, He of the Three-horned Face. <br/> <i>From a statuette by Charles R. Knight.</i></div>
<p>To make these dry bones live again, to
clothe them with flesh and reconstruct the
<span class="pagenum"><SPAN name="Page_127">[127]</SPAN></span>
creature as he was or may have been in life,
is, to be honest, very largely guesswork,
though to make a guess that shall come anywhere
near the mark not only demands a
thorough knowledge of anatomy—for the
basis of all restoration must be the skeleton—but
calls for more than a passing acquaintance
with the external appearance of living animals.
And while there is nothing in the bones to
tell how an animal is, or was, clad, they will at
least show to what group the creature belonged,
and, that known, there are certain
probabilities in the case. A bird, for example,
would certainly be clad in feathers. Going a
little farther, we might be pretty sure that
the feathers of a water-fowl would be thick
and close; those of strictly terrestrial birds,
such as the ostrich and other flightless forms,
lax and long. These as general propositions;
of course, in special cases, one might easily
come to grief, as in dealing with birds like
penguins, which are particularly adapted for
an aquatic life, and have the feathers highly
modified. These birds depend upon their fat,
and not on their feathers, for warmth, and so
<span class="pagenum"><SPAN name="Page_128">[128]</SPAN></span>
their feathers have become a sort of cross between
scales and hairs. Hair and fur belong
to mammals only, although these creatures
show much variety in their outer covering.
The thoroughly marine whales have discarded
furs and adopted a smooth and slippery skin,<SPAN name="FNanchor_9_9"></SPAN><SPAN href="#Footnote_9_9" class="fnanchor">[9]</SPAN>
well adapted to movement through the water,
relying for warmth on a thick undershirt of
blubber. The earless seals that pass much of
their time on the ice have just enough hair
to keep them from absolute contact with it,
warmth again being provided for by blubber.
The fur seals, which for several months in the
year dwell largely on land, have a coat of fur
and hair, although warmth is mostly furnished,
or rather kept in, by fat.</p>
<div class="footnote"><p><SPAN name="Footnote_9_9"></SPAN><SPAN href="#FNanchor_9_9"><span class="label">[9]</span></SPAN> <i>The reader is warned that this is a mere figure of speech,
for, of course, the process of adaptation to surroundings is
passive, not active, although there is a most unfortunate tendency
among writers on evolution, and particularly on mimicry,
to speak of it as active. The writer believes that no animal
in the first stages of mimicry, consciously mimics or endeavors
to resemble another animal or any part of its surroundings,
but a habit at first accidental may in time become
more or less conscious.</i></p>
</div>
<p>No reptile, therefore, would be covered with
<span class="pagenum"><SPAN name="Page_129">[129]</SPAN></span>feathers, neither, judging from those we
know to-day, would they be clad in fur or
hair; but, such coverings being barred out,
there remain a great variety of plates and
scales to choose from. Folds and frills, crests
and dewlaps, like beauty, are but skin deep,
and, being thus superficial, ordinarily leave no
trace of their former presence, and in respect
to them the reconstructor must trust to his
imagination, with the law of probabilities as a
check rein to his fancy. This law would tell us
that such ornaments must not be so placed as
to be in the way, and that while there would be
a possibility—one might even say probability—of
the great, short-headed, iguana-like
Dinosaurs having dewlaps, that there would
be no great likelihood of their possessing ruffs
such as that of the Australian Chlamydosaurus
(mantled lizard) to flap about their ears.
Even Stegosaurus, with his bizarre array of
great plates and spines, kept them on his
back, out of the way. Such festal ornamentation
would, however, more likely be found in
small, active creatures, the larger beasts contenting
themselves with plates and folds.</p>
<p><span class="pagenum"><SPAN name="Page_130">[130]</SPAN></span></p>
<p>Spines and plates usually leave some trace
of their existence, for they consist of a super-structure
of skin or horn, built on a foundation
of bone; and while even horn decomposes
too quickly to "petrify," the bone will
become fossilized and changed into enduring
stone. But while this affords a pretty sure
guide to the general shape of the investing
horn, it does not give all the details, and there
may have been ridges and furrows and sculpturing
that we know not of.</p>
<p>Knowing, then, what the probabilities are, we
have some guide to the character of the covering
that should be placed on an animal, and if
we may not be sure as to what should be done,
we may be pretty certain what should not.</p>
<p>For example, to depict a Dinosaur with
smooth, rubbery hide walking about on dry
land would be to violate the probabilities, for
only such exclusively aquatic creatures as the
whales among mammals, and the salamanders
among batrachians, are clothed in smooth,
shiny skin. There might, however, be reason
to suspect that a creature largely aquatic in its
habits did occasionally venture on land, as, for<span class="pagenum"><SPAN name="Page_131">[131]</SPAN></span>
instance, when vertebræ that seem illy adapted
for carrying the weight of a land animal are
found in company with huge limb-bones and
massive feet we may feel reasonably certain
that their owner passed at least a portion of his
time on <i>terra firma</i>.</p>
<p>So much for the probabilities as to the covering
of animals known to us only by their fossil
remains; but it is often possible to go beyond
this, and to state certainly how they were
clad. For while the chances are small that
any trace of the covering of an extinct animal,
other than bony plates, will be preserved, Nature
does now and then seem to have relented,
and occasionally some animal settled to rest
where it was so quickly and quietly covered
with fine mud that the impression of small
scales, feathers, or even smooth skin, was preserved;
curiously enough, there seems to be
scarcely any record of the imprint of hair.
Then, too, it is to be remembered that while
the chances were very much against such preservation,
in the thousands or millions of times
creatures died the millionth chance might come
uppermost.</p>
<p><span class="pagenum"><SPAN name="Page_132">[132]</SPAN></span></p>
<p>Silhouettes of those marine reptiles, the Ichthyosaurs,
have been found, probably made by
the slow carbonization of animal matter, showing
not only the form of the body and tail, but
revealing the existence of an unsuspected back
fin. And yet these animals were apparently
clad in a skin as thin and smooth as that of a
whale. Impressions of feathers were known
long before the discovery of Archæopteryx; a
few have been found in the Green River and
Florissant shales of Wyoming, and a Hesperornis
in the collection of the State University
of Kansas shows traces of the existence of
long, soft feathers on the legs and very clear
imprints of the scales and reticulated skin that
covered the tarsus. From the Chalk of Kansas,
too, came the example of Tylosaur, showing
that the back of this animal was decorated
with the crest shown in Mr. Knight's restoration,
one not unlike that of the modern iguana.
From the Laramie sandstone of Montana Mr.
Hatcher and Mr. Butler have obtained the impressions
of portions of the skin of the great
Dinosaur, Thespesius, which show that the
covering of this animal consisted largely, if not<span class="pagenum"><SPAN name="Page_133">[133]</SPAN></span>
entirely, of small, irregularly hexagonal horny
scutes, slightly thickened in the centre. The
quarries of lithographic stone at Solenhofen
have yielded a few specimens of flying reptiles,
pterodactyls, which not only verify the correctness
of the inference that these creatures possessed
membranous wings, like the bats, but
show the exact shape, and it was sometimes
very curious, of this membrane. And each and
all of these wonderfully preserved specimens
serve both to check and guide the restorer
in his task of clothing the animal as it was in
life.</p>
<p>And all this help is needed, for it is an easy
matter to make a wide-sweeping deduction,
apparently resting on a good basis of fact, and
yet erroneous. Remains of the Mammoth
and Woolly Rhinoceros, found in Siberia and
Northern Europe, were thought to indicate
that at the period when these animals lived
the climate was mild, a very natural inference,
since the elephants and rhinoceroses we now
know are all inhabitants of tropical climes.
But the discovery of more or less complete
specimens makes it evident that the climate<span class="pagenum"><SPAN name="Page_134">[134]</SPAN></span>
was not particularly mild; the animals were
simply adapted to it; instead of being naked
like their modern relatives, they were dressed
for the climate in a woolly covering. We
think of the tiger as prowling through the
jungles of India, but he ranges so far north
that in some localities this beast preys upon
reindeer, which are among the most northern
of large mammals, and there the tiger is clad
in fairly thick fur.</p>
<p>When we come to coloring a reconstructed
animal we have absolutely no guide, unless we
assume that the larger a creature the more soberly
will it be colored. The great land animals
of to-day, the elephant and rhinoceros, to
say nothing of the aquatic hippopotamus, are
very dully colored, and while this sombre coloration
is to-day a protection, rendering these
animals less easily seen by man than they
otherwise would be, yet at the time this color
was developing man was not nor were there
enemies sufficiently formidable to menace the
race of elephantine creatures.</p>
<p>For where mere size furnishes sufficient protection
one would hardly expect to find protective<span class="pagenum"><SPAN name="Page_135">[135]</SPAN></span>
coloration as well, unless indeed a
creature preyed upon others, when it might be
advantageous to enable a predatory animal to
steal upon its prey.</p>
<p>Color often exists (or is supposed to) as a
sexual characteristic, to render the male of a
species attractive to, or readily recognizable
by, the female, but in the case of large animals
mere size is quite enough to render them conspicuous,
and possibly this may be one of the
factors in the dull coloration of large animals.</p>
<p>So while a green and yellow Triceratops
would undoubtedly have been a conspicuous
feature in the Cretaceous landscape, from what
we know of existing animals it seems best to
curb our fancy and, so far as large Dinosaurs
are concerned, employ the colors of a Rembrandt
rather than those of a sign painter.</p>
<p>Aids, or at least hints, to the coloration of
extinct animals are to be found in the coloration
of the young of various living species, for
as the changes undergone by the embryo are
in a measure an epitome of the changes undergone
by a species during its evolution, so the
brief color phases or markings of the young<span class="pagenum"><SPAN name="Page_136">[136]</SPAN></span>
are considered to represent the ordinary coloring
of distant ancestors. Young thrushes are
spotted, young ostriches and grebes are irregularly
striped, young lions are spotted, and in
restoring the early horse, or Hyracothere, Professor
Osborn had the animal represented as
faintly striped, for the reason that zebras, the
wild horses of to-day, are striped, and because
the ass, which is a primitive type of horse, is
striped over the shoulders, these being hints
that the earlier horse-like forms were also
striped.</p>
<p>Thus just as the skeleton of a Dinosaur may
be a composite structure, made up of the
bones of a dozen individuals, and these in turn
mosaics of many fragments, so may the semblance
of the living animal be based on a fact,
pieced out with a probability and completed
by a bit of theory.</p>
<h3><i>REFERENCES</i></h3>
<p><i>There is a large series of restorations of extinct animals,
prepared by Mr. Charles R. Knight, under the
direction of Professor Osborn, in the Hall of Palæontology
of the American Museum of Natural History,<span class="pagenum"><SPAN name="Page_137">[137]</SPAN></span>
and these are later to be reproduced and issued in portfolio
form.</i></p>
<p><i>Should the reader visit Princeton, he may see in the
museum there a number of B. Waterhouse Hawkins's
creations—creations is the proper word—which are of
interest as examples of the early work in this line.</i></p>
<p><i>The "Report of the Smithsonian Institution for
1900" contains an article on "The Restoration of
Extinct Animals," pages 479-492, which includes a
number of plates showing the progress that has been
made in this direction.</i></p>
<div class="figcenter"> <ANTIMG src="images/i_184.jpg" width-obs="400" height-obs="179" alt="" /> Fig. 27.—A Hint of Buried Treasures.</div>
<hr class="chapter" />
<p><span class="pagenum"><SPAN name="Page_138">[138]</SPAN></span></p>
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